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- W2357676979 abstract "The infulence of sediment-laden flow on bed material composition of the active layer in the process of degradation and aggreagtion are considered to be composed of two parts with different sacle and mechanism. One is the turbulence burst taken place on the bed surface inducing the exchange between the sediment carried by flow and those setting on the bed surface. The other is the periodical deformation of the bed forms, especially the sand waves, which causes the mixing of bed material within the active layer. The equation describing these two processes is derived on the basis of mass conservation in the active layer.The variables of the equation are decomposed into two parts, one is corresponding to the average movement of sediment in active layer and the other one is corresponding to the disturbance due to bed form deformation.This partical difference equation appears to be a diffusion equation with source term.The application of the proposed equation to a simplified case of bed degradation is presented.The result shows it is reasonable." @default.
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- W2357676979 date "2004-01-01" @default.
- W2357676979 modified "2023-09-28" @default.
- W2357676979 title "Basic equation for variation of bed material composition in active layer of alluvial river" @default.
- W2357676979 hasPublicationYear "2004" @default.
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